Abstract. Large volume detectors such as IceCube, designed for the detection of astrophysical neutrinos register cosmic ray-induced atmospheric muon bundles at a rate of several thousand events per second. Due to the large amount of surrounding material, the effective energy threshold for muons reaching the detector typically lies at approximately one TeV. Through careful evaluation of event profiles it is possible to address cosmic ray and particle physics issues in an unprecedented energy region. Results from the analysis of one year of IceCube data are presented and their implications discussed.
IntroductionFor underground detectors placed within mountains or below earth or sea level, the amount of material between the surface and the instrumented volume is of the order of several thousand tons per square meter. The only charged particles produced in cosmic ray air showers remaining at detector depth are muons, and even for these the energy threshold lies in the TeV region.Large-volume underground detectors have for a long time been used for cosmic ray physics. The most common and simplest measurement is the zenith angle distribution of atmospheric muons. Although the exact functional form depends on the geometry of the surrounding material, the distance that particles have to traverse before reaching the detector usually increases towards the horizon as a function of the zenith angle θ zen . The muon energy spectrum can be derived by relating threshold energy to the varying distance between surface and detector. Measurements during the early 1990s, summarized in [1], often showed significant excesses over model predictions, a situation that was rectified in 1998 by the LVD collaboration [2], who demonstrated that the muon flux was in fact consistent with air shower simulations based on a primary nucleon flux following a simple power law of the form E −2.78±0.05 .The IceCube array, designed primarily for the detection of astrophysical neutrinos, is the first particle detector with an instrumented volume of the order of a cubic kilometer [3]. The consequent increases in effective area and observable track length represent a significant qualitative advance for the study of cosmic ray physics. In recognition of this fact, the underground detector was complemented with the surface array IceTop, whose primary stated purpose is to measure the electromagnetic component of air showers in coincidence with highenergy muon bundles traversing the main detector volume [4].